THE HISTORY of the VEGETATION and CLIMATE in SOUTHERN TASMANIA SINCE the LATE'-PLEISTOCENE • (..- A.•13.000 - 0 BP)
Total Page:16
File Type:pdf, Size:1020Kb
THE HISTORY OF THE VEGETATION AND CLIMATE IN SOUTHERN TASMANIA SINCE THE LATE'-PLEISTOCENE • (..- a.•13.000 - 0 BP) by MICHAEL MACPHAIL . BSc. (H6ns) Sydney. submitted in fulfilment of the requirements for - the degree of DOCTOR OF PHILOSOPHY • w2--- UNIVERSITY OF TASMANIA HOBART (November 1975).. VOLUME. TWO APPENDICES, BIBLIOGRAPHY, MAPS, FIGURES AND SUPPORTING PAPERS 1 . APPENDIX 1. CONTEMPORARY ACCOUNT OF THE APPARENT EFFECTS OF "THE .GAT FROST" OF.1837. "The road to Marlborough passes across the southern edge of this valley; it is then directed through a succession of forests and beautiful little marshes (amongst the latter are the Duck and Boggy Marshes), all of which are very fertile. _The excellence of most of the pasture and the frequent occurrence of these handsome plains or marshes in the Midst of the woods, give. a pleasing character to the bush here, which is always welcome. A walk of about six miles from Victoria. Valley places us on the bridge of the Dee, which is in this part a rather sluggish river, perhaps twenty yards wide, formed by the overflowings of Lake Echo. It is at this part of the journey that we catch the first sight, of the effects of the rigorous winter of 1837, a season of extraordinary severity, and which in a few weeks struck with death the forests throughout the valleys of well near all the highlands of this part of Tasmania. Here, however, it ceased its ravages, and its withering march from the westward was stayed. The storm moderated and when it reached this river it seems to have wholly died away, but not before its task was finished, its work of dem- olition fully completed; for the destruction of the forests ofall the lowlands, of this extensive district could not have been more perfectly accomplished if even a simoom had passed over them- This extraordinary season destroyed the timbcr of almost every valley on the vast plateau lying between this quarter and the mountains terminating at the verge of the Westbury and Norfolk Plains districts. The havoc has been indeed tremendous, but wholly incalculable. It is impossible to witness the effects of this winter without emotion and the traveller unaccustomed to such a picture of desolation is startled at the amazing scene of ruin which now presents itself. The bush is one interminable mass of dead trees. Except on the hill tops everything around him is dead. Whichever way he looks he sees hardly anything but dead forests, one apparently endless expanse of dead trees. The further he advances beyond the Dee, the more perfect has been the destruction. About this river, where the tempest seems to have.slackened, nearly half the trees have perished, or are only now recovering the shock they received thirteen years ago. But it is around, the incipient tuwa of Marlborough that the winter seems to have put forth its full strength, for here (the hill tops always excepted) the annihilation of life is almost universal; for miles every tree on the loWer•lands had died. A person writing of the districts I have undertaken to describe will not be accused of digressing in pausing to attempt the . investigation of the cause which led to the demolition, Of the forests here. The subject is interesting, and that task can never be considered an unprofitable one which has for its object the exposition of the truth; and, if possible, the correction of the vague hypothesis br which some have endeavoured to account for their decay - I believe, more with the view Of establishing new theories than of coming at the truth. According to some this was occasioned by disease; to others. , by lightning; while another class ascribe the calamity to extensive bush fires. But these persons are either ignorant Of the true cause, or they belong to that class of men who will never adopt a common- sense view of anything. I was a traveller in these districts as long ago as .1835. At that time the trees were everywhere, fresh and vigorous. In the beginning of 1838 I passed this way again, only a few months after the destruction of these forests had been effected, The ground was then covered with dead leaves, * It is very extraordinary fact, that within the last year or two about four of the trees in this township have put forth leaves after an apparent suspension of vitality of ten or eleven years' duration. (the effect of the simultaneous decay of the millions of trees which had just perished), and the bark was hanging in shreds from every bough. A most severe winter had occurred not long before', and a deep snow had fallen, which lay on the ground for many weeks, by which (the grasses excepted) vegetation on the lower lands was perfectly annihilated. The kangaroos, which swarmed here in '35, were all but extinguished; and one of a party of men who was up here then assured me that by taking advantage of the helpless condition to which the poor animals were reduced by hunger and long-continued cold, he and some others killed, in one afternoon, no less a number than sixty-seven. Judging from the quantities of their bones which found scattered everywhere, (I am speaking of '38), they must have died by thousands. If we did net know that the destruction of the trees took place with the occurrence of this terrible winter, an examination of the district would lead us to infer that cold was the agent, from the simple fact, that on the top of every hill and every ridge the trees never died. This is to be seen everywhere, even around Marlborough about which place the winter appears to have poured the full storm of its strength. It is not on one hill top alone that the trees are still green and vigorous but on every hill throughout the district. If, then, fire were really the agent, how came the trees to have escaped death in these situations, and that invariably? Are its effects less destructive on the hills than elsewhere? The answer of every one will be, certainly not. Again, do bush fires destroy the forests, or even seriously injure them? We see the contrary in five hundred cases every summer; and if such were the case, there ought not to be a tree left us in all Tasmania. But the notion is absurd. Moreover, the trees in these districts do not exhibit any extraordinary marks of fire as would certainly be the case had they beendestroyed by it. But I believe we might as well impute the devast- ation to the Mosaic deluge as to either fire or disease." Extract from J. E. Calder. ''Some account of the Country. between Hamilton and the Frenchmans Cap". Hobart Town Courier, 21st September 1850 1 . APPENDIX 2 The Preparation of Fossil Pollen Extracts from Late Quaternary Sediments in Tasmania. A. Equipment Used (six samples processed concurrently). 1. 12 x 15 ml. round bottom glass "SE" centrifuge tubes (heat resistant), 0..6 inch external diameter. 2. 6 x 15 ml. plastic "MSE" centrifuge tubes, 0.6 inch external diameter. 3. 12 x "Oxoid" irdcrobiclogical caps to fit glass centrifuge tubes.. 4. 1 x roll of "Parafilm" (for sealing the plastic centrifuge tubes). 5. 6 x 45 ml. plastic "MSE" centrifuge tubes, 1.2 inch external diameter. 6. 1 x "MSE MINOR CENTRIFUGE" (Code No. 1265) with two heads and tube holder sets: (i) a 'swing' head to hold the 0.6 inch tubes (glass tubes were found to break in a fixed angle head). (ii) a fixed angle head to hold the 1.2 inch tubes. 7. 6 x plastic wash bottles for dispensing reagents. 8. microbiological glass rod 'spreaders', disposable 'Pasteur" pipettes and assorted glass beakers, 50 - 500m1. 9. Glass slides. and 1/2 inch square No. 0 to 1 size coverslips (both stored in an 100:1 Ethanol: HC1 solution). 10. "Quikstik" permanent adhesive slide labels. 11. Variable heat setting hotplate. 12. Water bath and tube holders to fit both 0.6 and 1.2 inch centrifuge tubes. 13. "Beam" balance for balancing centrifuge tubes. 14. "Whirlimix" test tube stirrer. 15. "Endecott" 5 inch (or smaller) test seives, 250, 150 and, if required,. 100/Amesh sizes, lid and collecting basin to fit. 16. Reagents (all 'A.R.' grade) Hydrochloric acid Acetic Anhydride Hydrofluoric acid Glycerol 2. Sulphuric acid Saffranin Glacial Acetic acid - Potassium Hydroxide N.B. Access to either filtered de-ionized or distilled water and a well- equipped fume cupboard is essential as is the use of rubber gloves in handling most of the above reagents. 17. Make up: (i) 10% w/v KOH solution. (ii) 9:1 Acetic Anhydride: conc. Sulphuric acid solution (mixture should be made up fresh for each preparation. This "Acetolysis" mixture explodes on contact with water). (iii) Saffranin solution. Enough is dissolved in distilled water to give A med.. rose colour . (a deep 'claret' coloured solution is too con- centrated). B. Extractive Procedures. 0.2 gm. of oven dried material is sufficient except in the case of glacifluvial clays. Here, up to 2 gm. may be required. :#* (a) Lacustrine Clays (b) Clay-free Peats 1. .test for the presence of break up peat gently and soak overnight• carbonates using HC1. in ca. 5m1. 10% KOH in a small glass centri- fuge tube.Seal. using "Parafilm'. Any sand in the peat can then be .removed by a series of decants of the KOH suspension. • 2. place .sediment in either "Whirlimix" to break up organic matcer a small or large plastic aggregates. centrifuge tube depending on clay content.